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42 Cards in this Set

  • Front
  • Back
the study of the occurrence, circulation, and distribution of water on Earth and in its atmosphere.
hydrology
sum of all rainwater on the surface
runoff
mass of water stored below the Earth’s surface. Water stored in rock and soil.
groundwater
portion of volume of a material that consists of open spaces
porosity
measure of the speed at which fluid can travel through a porous medium. How connected pore spaces are.
permeability
portion of soil and rock near the surface in which open spaces are filled primarily with air (aka unsaturated zone)
zone of aeration
zone in which pore spaces are filled with air
saturated zone
boundary between zone of aeration and saturated zone
groundwater table
infiltration of water into the subsurface
recharge
opposite of recharge-release of groundwater to the surface
discharge
body of rock that is sufficiently water permeable to yield economically significant quantities to wells and springs
aquifer
body of relatively impermeable rock that is capable of absorbing water slowly but does not transmit it rapidly enough to supply a well or spring.
aquiclude
locations where the water table intersects the ground
springs
overpumping leads to Cone of Depression and salt water is drawn in
saltwater intrusion
body of water flowing in a channel. The floor of the channel is called the bed
stream
area of land surrounded by topographic divides in which all the water is directed to a single point
drainage basin
cross-sectional view or profile of a river-the height of a riverbed at any point in its course
longitudinal profile
elevation at which a stream enters a large body of water such as a lake or ocean
base level
in which neither erosion nor deposition is occurring, due to an equilibrium of slope, velocity, and discharge
graded stream
cone shaped or fan-shaped accumulations at a steep slope change
alluvial fans
a material’s resistance to flow. Higher viscosity=slower flowing
viscosity
fluid moves in straight lines or slightly curved paths. Streamlines do not cross
laminar flow
irregular, swirling flow, streamlines cross, occurs at most rates of stream flow, keeps smaller particles in suspension
turbulent flow
total amount of water that passes a given point in a stream per unit of time
discharge
location of a significant sedimentation where a river meets the sea
delta
natural flow of air that is parallel to the surface of a rotating planet
wind
geological processes driven by wind
Eolian
in the NORTHERN hemisphere, currents are to the right (clockwise), in the SOUTHERN hemisphere, currents are to the left (counterclockwise)
Coriolis effect
blanket of sediment composed of fine-grained particles
loess
permanent or temporary lakes that occur in mountain valleys or basins
Playa lake
body of ice, snow, firn, and meltwater, lying wholly or mostly on land, showing evidence of present or former motion
glacier
Accumulation < ablation
glacier front recedes
accumulation > ablation
glacier front advances
restricted to mountains
alpine glaciers
cover extremely large areas
continental glaciers
scraping of scratching of bedrock material by ice (brittle)
abrasion
entrainment of fractured bedrock into the ice
plucking
an amphitheater-like hollow, usually shaped like half of an inverted cone, formed at the head of a glacial valley by the plucking and tearing action of ice
cirque
ridges of till deposited at cert places in glaciers (end, lateral, medial)
moraine
large, streamlined hill of till and bedrock that parallels the past direction of glacial movement
drumlin
long, narrow, winding ridges of sand, can be Km long, roughly parallel to the direction of ice movement, deposited by meltwater streams exiting the base of the glacier
esker
the shape of Earth’s orbit around the Sun
eccentrity